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The thermal springs of Bath

Andrews, JN; Burgess, WG; Edmunds, WM; Kay, RLF; Lee, DJ; (1982) The thermal springs of Bath. Nature , 298 pp. 339-343. 10.1038/298339a0.

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Abstract

Geochemical and hydrogeological evidence shows that the thermal springs at Bath originate from the Mendip Hills. A maximum subsurface temperature of 80 +/- 16 °C is attained during circulation to between 2.7 and 4.3 km within the Carboniferous Limestone. The residence time of the bulk of the water is <10,000 yr.

Type: Article
Title: The thermal springs of Bath
DOI: 10.1038/298339a0
UCL classification: UCL > Provost and Vice Provost Offices
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: http://discovery.ucl.ac.uk/id/eprint/169448
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